Appendix/Ramblings/T3Integrals/QuadraticCase

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T3 Coordinates (continued)

On one accompanying wiki page we have introduced T3 Coordinates and on another we have described how Jay Call's Characteristic Vector applies to T3 Coordinates. Here we investigate the properties of our T3 Coordinate system in the special case when q2=2; Jay Call's independent analysis is recorded on a separate page.

Special Case (Quadratic)

Coordinate Relations

When q2=2, the two key coordinates are:

λ1

=

ϖcoshZ

λ2

=

ϖsinhZ

Note also:   

X2λ1λ2

=

2sinhZcoshZ=sinh(2Z),

where, in this case,

Zsinh1(2zϖ).

For this special case, we can invert these coordinate relations to obtain analytic expressions for both ϖ and z in terms of λ1 and λ2. Specifically, the relation,

1=cosh2Zsinh2Z=(λ1ϖ)2(ϖλ2)2

implies that the function ϖ(λ1,λ2) can be obtained from the physically relevant root of the following equation:

ϖ4λ22+ϖ2λ12=0.

The relevant root gives,

ϖ2=λ222[1+(2λ1/λ2)21]=λ222[cosh(2Z)1]

ϖ=λ22[cosh(2Z)1]1/2.

The desired function z(λ1,λ2) is therefore,

z=ϖ2sinhZ=ϖ22λ2=λ222[1+(2λ1/λ2)21]

z=12λ22[cosh(2Z)1].

In an effort to simplify the appearance of these and future expressions, we will henceforth adopt the notation,

Λcosh(2Z)Λ=1+X2.

In terms of Λ, then, we have,

ϖ

=

λ22[Λ1]1/2;

z

=

12λ22[Λ1].


Scale Factor Expressions

We are now in a position to express the two key scale factors purely in terms of the two key T3 coordinates. First, we note that,

2=[ϖ2+4z2]1=2λ22(Λ1)Λ,

and,

(λ1λ2)2=14X2=14(Λ21)=14(Λ1)(Λ+1).

Hence,

h12

=

λ122

=

12[Λ+1Λ];

h22

=

(q21)(ϖzλ2)2

=

18(Λ1)2Λ.

We note also that,

dΛdt

=

ddt[1+(2λ1/λ2)2]1/2

=

[Λ21Λ]dln(λ1/λ2)dt.

Hence, starting from the general expression for dlnh2/dt derived elsewhere, we deduce that,

dlnh2dt

=

2h14ddt[ln(λ1/λ2)]

=

12(Λ+1Λ)2[Λ21Λ]1dΛdt

=

12(Λ+1Λ1)dlnΛdt.

(This identical expression also can be derived straightforwardly from the specific expression for h2 given above.) From the expression given above for h1, we also deduce that,

dlnh1dt=12(Λ+1)dlnΛdt.

As a check, we note that the relationship between dlnh1/dt and dlnh2/dt in this specific case (i.e., q2=2) matches the general relationship between these two logarithmic time-derivatives that has been derived elsewhere, namely,

(h1λ1)2dlnh1dt+(h2λ2)2dlnh2dt=0.

Equation of Motion

According to Equation EOM.01, as derived elsewhere in the context of T3 coordinates, a general expression for the second component of the equation of motion is,

d(h2λ˙2)dt=(λ2λ˙1λ1)dh2dt

λ¨2λ2=[λ˙1λ1λ˙2λ2]dlnh2dt=[dln(λ1/λ2)dt]dlnh2dt.

Based on the derivations provided above, both factors that make up the term on the RHS of this expression can be written entirely in terms of the variable, Λ. This allows us to rewrite Equation EOM.01 as,

λ¨2λ2=[ΛΛ21dΛdt][12Λ(Λ+1Λ1)dΛdt]=12(Λ1)2[dΛdt]2

T3Q.01

2λ¨2λ2=[dln(Λ1)dt]2.

Solution Strategy

I'm not sure whether the following strategy is fully legitimate, but let's explore it anyway. Because the LHS of Equation T3Q.01 displays an explicit dependence only on the coordinate λ2 while the RHS displays an explicit dependence only on Λ — that is, only on the ratio of the two coordinates λ1/λ2 — perhaps we can use a separation of variables technique to derive a solution. Specifically, suppose the LHS and the RHS separately are set equal to the same value, call it n.

Then, for the LHS:

λ¨2=n2λ2;

And, for the RHS:

dln(Λ1)dt=n.

Now I suppose that, in general, n should be allowed to vary with time, but for exploratory purposes, let's assume that n is a constant. The solution to the LHS's 2nd-order ODE is,

λ2=λ20exp[n/2t],

where, λ20 is the coordinate position λ2 at time t=0. The solution to the RHS's 1st-order ODE is,

nt=ln(Λ1Λ01),

where, Λ0 is given by the coordinate ratio at time t=0, specifically, Λ01+(2λ10/λ20)2.

Now, if we replace "nt" in the first of these expressions by the second expression, we find,

λ2λ20=exp[12ln(Λ1Λ01)]=(Λ01Λ1)1/2.

This would be a fantastically simple result, if it proved to be a proper solution to the governing equation of motion. Unfortunately, if this relatively elementary equation is differentiated twice in an effort to reproduce Equation T3Q.01, we find that an additional undesirable term appears that involves the second derivative of a function containing the variable Λ. It can be shown that this undesirable term goes to zero if n is assumed to be independent of time (as we did indeed assume, above). Unfortunately, in reality, this does not seem to be a desirable assumption for the physical problem in which we have interest, so we must conclude that the derived elementary equation is not the desired solution of the equation of motion.

But can we learn something valuable from this failed separation of variables approach???

Another Thought

It can easily be shown that, in general,

ddt(F˙F)=F¨F[dlnFdt]2.

Hence, Equation T3Q.01 can be rewritten as,

ddt(λ2˙λ2)+[dlnλ2dt]2=[dln(Λ1)1/2dt]2

ddt(dlnλ2dt)=[dln(Λ1)1/2dt]2[dlnλ2dt]2=[dln(Λ1)1/2dt+dlnλ2dt][dln(Λ1)1/2dtdlnλ2dt]

ddt(dlnλ2dt)=dln[(Λ1)1/2λ2]dtdln[(Λ1)1/2λ21]dt

Can we gain any insight from this form of the 2nd component of the equation of motion? For example, can the convert the RHS into the total time-derivative of some function?

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